A mid level short wave impulse and a surface frontal boundary acted together to trigger late afternoon and early evening thunderstorms over western and north central North Dakota on June 24th. The most intense storms developed across southwest North Dakota where the strongest low level wind shear and moisture pooling were collocated. One of the longer tracked supercell storms spawned two distinct and seperate tornadoes. One of those resulted in EF1 tornado damage on a farm. Numerous reports of severe hail and two reports of severe thunderstorm wind gusts were received in addition to tornado and funnel cloud reports.